Mini TO TPS Bahasa Inggris 1

1. Le Mans is … and has factories that produce automobiles, aircraft, chemicals, textiles, and tobacco products.

2. The French … Marius Petipa was responsible for building the classic ballet in Russia.

3. Shanghai … on a flat coastal plain south of the mouth of the Yangtze River, on the tidal Whangpoo River not far from the coast.

4. Acute leukemias are usually fatal within a period … to one to two years.

5. It is not certain … traffic congestion in Jakarta.

Text 1 (for Questions 6–10)

Aurora is a natural display of light in the sky that can be seen with the unaided eyes only at night. An aurora display in the Northern Hemisphere is called the aurora borealis, or the northern lights. A similar phenomenon in the Southern Hemisphere is called the aurora australis. Auroras are the most visible effect of the sun’s activity on the earth’s atmosphere. Most auroras occur in far northern and southern regions. They appear chiefly as arcs, clouds, and streaks. Some move, brighten, or flicker suddenly. The most common color in an aurora is green but displays that occur extremely high in the sky may be red or purple. Most auroras occur about 60 to 620 miles (97 to 1,000 kilometers) above the earth. Some extend lengthwise across the sky for thousands of miles or kilometers.

Auroral displays are associated with the solar wind, a continuous flow of electrically charged particles from the sun. When these particles reach the earth’s magnetic field, some get trapped. Many of these particles travel toward the earth’s magnetic poles. When the charged particles strike atoms and molecules in the atmosphere, energy is released. Some of this energy appears in the form of auroras.

Auroras occur most frequently during the most intense phase of the 11-year sunspot cycle. During this phase, dark patches on the sun’s surface, called sunspot increase in number. Violent eruptions on the sun’s surface, known as solar flares, are associated with sunspots. Electrons and protons released by solar flares add to the number of solar particles that interact with the earth’s atmosphere. This increased interaction produces extremely bright auroras. It also results in sharp variations in the earth’s magnetic field called magnetic storms. During these storms, auroras may shift from the polar regions toward the equator.

6. The author’s purpose in writing this text is …

Text 1 (for Questions 6–10)

Aurora is a natural display of light in the sky that can be seen with the unaided eyes only at night. An aurora display in the Northern Hemisphere is called the aurora borealis, or the northern lights. A similar phenomenon in the Southern Hemisphere is called the aurora australis. Auroras are the most visible effect of the sun’s activity on the earth’s atmosphere. Most auroras occur in far northern and southern regions. They appear chiefly as arcs, clouds, and streaks. Some move, brighten, or flicker suddenly. The most common color in an aurora is green but displays that occur extremely high in the sky may be red or purple. Most auroras occur about 60 to 620 miles (97 to 1,000 kilometers) above the earth. Some extend lengthwise across the sky for thousands of miles or kilometers.

Auroral displays are associated with the solar wind, a continuous flow of electrically charged particles from the sun. When these particles reach the earth’s magnetic field, some get trapped. Many of these particles travel toward the earth’s magnetic poles. When the charged particles strike atoms and molecules in the atmosphere, energy is released. Some of this energy appears in the form of auroras.

Auroras occur most frequently during the most intense phase of the 11-year sunspot cycle. During this phase, dark patches on the sun’s surface, called sunspot increase in number. Violent eruptions on the sun’s surface, known as solar flares, are associated with sunspots. Electrons and protons released by solar flares add to the number of solar particles that interact with the earth’s atmosphere. This increased interaction produces extremely bright auroras. It also results in sharp variations in the earth’s magnetic field called magnetic storms. During these storms, auroras may shift from the polar regions toward the equator.

7. The word some in line 7 refers to …

Text 1 (for Questions 6–10)

Aurora is a natural display of light in the sky that can be seen with the unaided eyes only at night. An aurora display in the Northern Hemisphere is called the aurora borealis, or the northern lights. A similar phenomenon in the Southern Hemisphere is called the aurora australis. Auroras are the most visible effect of the sun’s activity on the earth’s atmosphere. Most auroras occur in far northern and southern regions. They appear chiefly as arcs, clouds, and streaks. Some move, brighten, or flicker suddenly. The most common color in an aurora is green but displays that occur extremely high in the sky may be red or purple. Most auroras occur about 60 to 620 miles (97 to 1,000 kilometers) above the earth. Some extend lengthwise across the sky for thousands of miles or kilometers.

Auroral displays are associated with the solar wind, a continuous flow of electrically charged particles from the sun. When these particles reach the earth’s magnetic field, some get trapped. Many of these particles travel toward the earth’s magnetic poles. When the charged particles strike atoms and molecules in the atmosphere, energy is released. Some of this energy appears in the form of auroras.

Auroras occur most frequently during the most intense phase of the 11-year sunspot cycle. During this phase, dark patches on the sun’s surface, called sunspot increase in number. Violent eruptions on the sun’s surface, known as solar flares, are associated with sunspots. Electrons and protons released by solar flares add to the number of solar particles that interact with the earth’s atmosphere. This increased interaction produces extremely bright auroras. It also results in sharp variations in the earth’s magnetic field called magnetic storms. During these storms, auroras may shift from the polar regions toward the equator.

8. Which of the following does solar wind in line 12 mean?

Text 1 (for Questions 6–10)

Aurora is a natural display of light in the sky that can be seen with the unaided eyes only at night. An aurora display in the Northern Hemisphere is called the aurora borealis, or the northern lights. A similar phenomenon in the Southern Hemisphere is called the aurora australis. Auroras are the most visible effect of the sun’s activity on the earth’s atmosphere. Most auroras occur in far northern and southern regions. They appear chiefly as arcs, clouds, and streaks. Some move, brighten, or flicker suddenly. The most common color in an aurora is green but displays that occur extremely high in the sky may be red or purple. Most auroras occur about 60 to 620 miles (97 to 1,000 kilometers) above the earth. Some extend lengthwise across the sky for thousands of miles or kilometers.

Auroral displays are associated with the solar wind, a continuous flow of electrically charged particles from the sun. When these particles reach the earth’s magnetic field, some get trapped. Many of these particles travel toward the earth’s magnetic poles. When the charged particles strike atoms and molecules in the atmosphere, energy is released. Some of this energy appears in the form of auroras.

Auroras occur most frequently during the most intense phase of the 11-year sunspot cycle. During this phase, dark patches on the sun’s surface, called sunspot increase in number. Violent eruptions on the sun’s surface, known as solar flares, are associated with sunspots. Electrons and protons released by solar flares add to the number of solar particles that interact with the earth’s atmosphere. This increased interaction produces extremely bright auroras. It also results in sharp variations in the earth’s magnetic field called magnetic storms. During these storms, auroras may shift from the polar regions toward the equator.

9. What type of information is included in the third paragraph?

Text 1 (for Questions 6–10)

Aurora is a natural display of light in the sky that can be seen with the unaided eyes only at night. An aurora display in the Northern Hemisphere is called the aurora borealis, or the northern lights. A similar phenomenon in the Southern Hemisphere is called the aurora australis. Auroras are the most visible effect of the sun’s activity on the earth’s atmosphere. Most auroras occur in far northern and southern regions. They appear chiefly as arcs, clouds, and streaks. Some move, brighten, or flicker suddenly. The most common color in an aurora is green but displays that occur extremely high in the sky may be red or purple. Most auroras occur about 60 to 620 miles (97 to 1,000 kilometers) above the earth. Some extend lengthwise across the sky for thousands of miles or kilometers.

Auroral displays are associated with the solar wind, a continuous flow of electrically charged particles from the sun. When these particles reach the earth’s magnetic field, some get trapped. Many of these particles travel toward the earth’s magnetic poles. When the charged particles strike atoms and molecules in the atmosphere, energy is released. Some of this energy appears in the form of auroras.

Auroras occur most frequently during the most intense phase of the 11-year sunspot cycle. During this phase, dark patches on the sun’s surface, called sunspot increase in number. Violent eruptions on the sun’s surface, known as solar flares, are associated with sunspots. Electrons and protons released by solar flares add to the number of solar particles that interact with the earth’s atmosphere. This increased interaction produces extremely bright auroras. It also results in sharp variations in the earth’s magnetic field called magnetic storms. During these storms, auroras may shift from the polar regions toward the equator.

10. The text indicates that …